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the stream found its new outlet and the branch cave had become
entirely filled; and when these processes were completed the floor of
the cave would be practically at its present level. Under the
circumstances exploration would probably, almost certainly, be
fruitless. The company which owns the cave would also wish it restored
to something like its present state.
ELLIS CAVE.--On the estate of Dr. Ellis, 19 miles north of Fort Payne
and 3 miles from Sulphur Springs, are two caves known locally as
Big-mouth and Little-mouth. The smaller is closed by a locked gate.
The larger has a rather imposing appearance from the outside. From a
ledge of rock, in place, in front of it, one looks down a steep slope
in which rocks up to 40 or 50 tons weight are imbedded. At a vertical
depth of 30 feet is a level space not more than 8 or 10 square yards
in area. From this a narrow crevice goes to the right. Within a few
yards it reaches a hole which can be descended only by means of a rope
or ladder. Persons have, however, gone several hundred yards in it.
On the left of the level space and bounded on each side by solid rock
walls is a pit 10 feet deep, caused by inflowing storm waters which
have created this depression in seeking a small outlet, also toward
the left. The height from the bottom of this sink to the roof of the
cave is nearly 50 feet.
Crossing this pit on a foot log, which rests on loose rock and earth
at its farther end, a crevice varying from 6 to 10 feet wide goes
inward for 50 feet. Earth covers the loose rock at the level of the
foot log almost at once, and this earth has a steep ascent toward the
rear. The crevice widens beyond the distance mentioned, though
irregularly, being in some places 25 feet from side to side. So far as
progress is concerned, the cave terminates 150 feet from the doorway
in a blank wall. It may be that if the earth were out of the way
further progress would be possible.
Considerable digging has been done for saltpeter, but except near the
front it has been only superficial.
The top of the earth at the extreme rear of the cave is almost or
quite as high as the roof at the front, which means that, if the
bottom should be level, the thickness of this accumulated deposit is
not less than 35 feet. As the dip is toward the rear and quite sharp,
about 10 or 12 degrees, the earth here may well be much thicker than
indicated.
Excavation would be tedious and costly, as it would be impos
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